Subduction zone intermediate-depth seismicity: Insights from the structural analysis of Alpine high-pressure ophiolite-hosted pseudotachylyte (Corsica, France)
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Alpine Corsica ophiolite pseudotachylyte formed in a subducting oceanic lithosphere.

Displacement sense associated with pseudotachylyte fault veins is determined.

Corsican ruptures are similar to seismic ruptures in Pacific plate beneath NE Japan.

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